Evans, Jeff; Dowdeswell, Julian A; Grobe, Hannes; Niessen, Frank; Stein, Ruediger; Hubberten, Hans-Wolfgang; Whittington, R J (2002): Grain size distribution of sediment core PS2628-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.58491, In supplement to: Evans, J et al. (2002): Late Quaternary sedimentation in Kejser Franz Joseph Fjord and the continental margin of East Greenland. Geological Society of London, Special Publications (Open Acess http://hdl.handle.net/10013/epic.15709.d008), 203, 149-179, https://doi.org/10.1144/GSL.SP.2002.203.01.09
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Evans, Jeff (2000): Late Weichselian and Holocene sedimentation in Kejser Franz Josephs Fjord and on the adjacent continental margin, East Greenland. PhD Thesis, Department of Earth Sciences, University of Cambridge, 150 pp
Project(s):
Funding:
Fourth Framework Programme (FP4), grant/award no. MAS3980185: Quaternary Environment of the Eurasian North
Coverage:
Latitude: 73.160000 * Longitude: -15.971660
Date/Time Start: 1994-09-03T12:05:00 * Date/Time End: 1994-09-03T12:05:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 2.20 m
Event(s):
PS2628-1 (PS31/136) * Latitude: 73.160000 * Longitude: -15.971660 * Date/Time: 1994-09-03T12:05:00 * Elevation: -1695.0 m * Penetration: 7 m * Recovery: 2.35 m * Location: East Greenland Sea * Campaign: ARK-X/2 (PS31) * Basis: Polarstern * Method/Device: Gravity corer (Kiel type) (SL) * Comment: 3 core sections: 0-0.35, 0.35-1.36, 1.36-2.35 m
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
264 data points
Data
1 Depth sed [m] | 2 >2 mm [%] | 3 Sand [%] | 4 Silt [%] | 5 <2 µm [%] | 6 2-1 mm [%] | 7 1-0.5 mm [%] | 8 500-250 µm [%] | 9 250-125 µm [%] | 10 125-63 µm [%] | 11 >50 µm [%] | 12 >40 µm [%] | 13 >30 µm [%] | 14 >20 µm [%] | 15 >16 µm [%] | 16 >14 µm [%] | 17 >12 µm [%] | 18 >10 µm [%] | 19 >8 µm [%] | 20 >6 µm [%] | 21 >4 µm [%] | 22 >2 µm [%] | 23 2-1 µm [%] | 24 <1 µm [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.01 | 0.00 | 8.58 | 50.01 | 41.42 | 0.422 | 1.476 | 1.054 | 2.073 | 3.549 | 0.549 | 3.657 | 4.206 | 8.78 | 3.931 | 1.737 | 2.377 | 3.02 | 4.023 | 3.57 | 5.211 | 8.96 | 12.525 | 28.89 |
0.20 | 0.00 | 13.00 | 48.00 | 39.00 | 0.073 | 0.146 | 0.439 | 3.948 | 8.394 | 0.000 | 39.00 | ||||||||||||
0.50 | 0.00 | 1.20 | 40.70 | 58.10 | 0.000 | 0.000 | 0.000 | 0.000 | 0.000 | 0.000 | 0.300 | 0.400 | 3.60 | 3.200 | 2.400 | 3.000 | 3.00 | 3.300 | 4.80 | 6.400 | 10.30 | 8.400 | 49.70 |
0.70 | 0.00 | 1.00 | 34.90 | 64.10 | 0.000 | 0.000 | 0.000 | 0.000 | 0.000 | 0.000 | 0.000 | 0.000 | 3.30 | 2.900 | 1.700 | 2.000 | 2.40 | 2.400 | 3.20 | 7.600 | 9.40 | 8.200 | 55.90 |
0.90 | 0.00 | 0.00 | 34.10 | 65.90 | 0.000 | 0.000 | 0.000 | 0.000 | 0.000 | 0.100 | 0.000 | 0.800 | 1.50 | 1.200 | 1.700 | 2.200 | 2.20 | 3.500 | 3.60 | 8.100 | 9.20 | 9.600 | 56.30 |
1.20 | 0.00 | 0.70 | 39.56 | 59.74 | 0.000 | 0.000 | 0.000 | 0.000 | 0.705 | 0.000 | 0.400 | 0.699 | 4.60 | 3.596 | 1.998 | 2.497 | 3.00 | 2.997 | 4.60 | 5.694 | 9.49 | 8.791 | 50.95 |
1.30 | 0.00 | 0.50 | 39.50 | 60.00 | 0.000 | 0.000 | 0.000 | 0.000 | 0.000 | 0.000 | 0.200 | 2.300 | 4.10 | 3.100 | 2.500 | 2.700 | 2.00 | 2.500 | 4.20 | 6.000 | 9.90 | 8.500 | 51.50 |
1.50 | 0.61 | 13.26 | 39.05 | 47.08 | 1.163 | 0.501 | 0.840 | 1.857 | 8.896 | 2.333 | 3.110 | 3.110 | 5.27 | 3.628 | 1.814 | 1.296 | 1.04 | 3.024 | 3.89 | 3.456 | 7.08 | 7.430 | 39.65 |
1.70 | 3.24 | 15.06 | 33.82 | 47.11 | 3.473 | 0.889 | 1.198 | 2.208 | 7.297 | 1.307 | 1.389 | 3.023 | 5.47 | 1.716 | 1.144 | 1.797 | 2.37 | 2.206 | 3.02 | 4.003 | 6.37 | 7.108 | 0.00 |
1.90 | 0.74 | 13.36 | 30.39 | 55.51 | 1.549 | 1.508 | 2.684 | 3.624 | 3.998 | 0.000 | 0.950 | 2.158 | 3.28 | 1.209 | 0.950 | 1.554 | 1.90 | 2.417 | 2.76 | 5.611 | 7.60 | 7.856 | 47.65 |
2.00 | 1.41 | 14.21 | 30.64 | 53.73 | 2.128 | 1.341 | 3.067 | 3.922 | 3.754 | 0.000 | 0.687 | 1.373 | 3.35 | 1.373 | 1.459 | 2.318 | 2.66 | 1.888 | 3.18 | 4.034 | 8.33 | 6.695 | 47.04 |
2.20 | 0.00 | 7.76 | 35.61 | 56.64 | 0.000 | 0.443 | 0.674 | 1.906 | 4.735 | 1.199 | 1.384 | 1.845 | 2.95 | 1.384 | 1.384 | 2.029 | 2.21 | 2.214 | 4.15 | 5.811 | 9.04 | 8.671 | 47.97 |